Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (3): 736-742.doi: 10.13278/j.cnki.jjuese.201503108

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Geochemical Characteristics and Genesis of the Oil Shale in Changle Sag,Shandong Province

Sun Yaoting1,2, Xu Shouyu1, Zhang Shiqi1, Xu Haoqing2, Guo Lili2   

  1. 1. School of Geosciences, China University of Petroleum(East China), Qingdao 266580, Shandong, China;
    2. Geo-Science Research Institute, Shengli Oilfield Company, SINOPEC, Dongying 257015, Shandong, China
  • Received:2014-10-12 Published:2015-05-26

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Abstract:

The oil shale of Changle sag exists in Lijiaya Formation of Wutu Group, corresponds to the stratum of 2nd Kongdian Formation in Jiyang depression and Weibei sag. By means of the organic geochemical theories and methods, the characteristics of oil shale in Changle sag are studied. The oil shale has a high organic matrix abundance. Its kerogen type is mainly typeⅠ and typeⅡ1, at an immature-low maturity stage, has a strong potential for oil generation,so it has good prospects for oil and gas exploration. By analyses of the regional tectonic evolution and climate change, the oil shale of Changle sag are formated in left turn to right turn conversion period of Tanlu fault zone, weak tectonic activity coupled with warm and humid climate. The oil shale and coal co-exist in TST and HST. The oil shale metallogenic model belongs to the rift lake march type.

Key words: Changle sag, oil shale, Lijiaya Formation, organic matrix, geochemistry, genesis, Shandong Province

CLC Number: 

  • P618.12

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